IB Chemistry Study Summary

Acids and Bases

1
Acid/Base Theory

Introduction to Acid-Base Theories

The understanding of acids and bases has evolved over time, leading to three primary definitions: Arrhenius, Brønsted-Lowry, and Lewis. Each theory offers a different perspective on the chemical behavior of these fundamental substances. The Arrhenius theory, developed by the Swedish chemist Svante Arrhenius in 1887, was the first formal definition. This was followed by the Brønsted-Lowry theory, independently published in 1923 by Lowry from England and Brønsted from Denmark. In the same year, the American chemist G.N. Lewis introduced an even broader definition, known as the Lewis theory, which is typically covered in Higher Level (HL) chemistry.

Arrhenius Theory of Acids and Bases

According to the Arrhenius definition, an acid is a substance that dissociates in water to produce hydrogen (H+) ions. Conversely, a base is a substance that dissociates in water to form hydroxide (OH-) ions. This theory recognized that hydrogen and hydroxide ions could combine to form water, and that the remaining cations and anions would form a salt. A significant limitation of the Arrhenius theory is its exclusive focus on aqueous systems, meaning it could not account for acid-base reactions occurring without water or involving insoluble bases. Interestingly, Arrhenius initially presented these ideas in his doctoral thesis, which was not well-received at the time, earning him only the lowest possible degree. However, his groundbreaking work was later recognized, and he was awarded the Nobel Prize in Chemistry in 1903. Arrhenius is also credited with being the first to predict global warming due to rising carbon dioxide levels.
Diagram

Understanding pH and pOH Scales

The pH scale is a measure of the acidity or alkalinity of an aqueous solution, defined by the negative logarithm of the hydrogen ion concentration, [H+]. Similarly, pOH is defined as the negative logarithm of the hydroxide ion concentration, [OH-]. These two scales are interconnected, with the sum of pH and pOH always equaling 14 at 298 K. This relationship is derived from the ion product of water, Kw, which is the product of the hydrogen and hydroxide ion concentrations. At 298 K, Kw is 1 × 10-14. Therefore, if a solution has a pH of 7, it is neutral, meaning [H+] = 1 × 10-7 M and [OH-] = 1 × 10-7 M. The formulas for these calculations are:
    • pH = -log[H+]
    • pOH = -log[OH
Diagram
-]
    • pH + pOH = 14
    • [H+] = 10-pH
    • [OH-] = 10-pOH
The dissociation constant of water, Kw, is given by the expression: [H+][OH-] = 1 × 10-14 = Kw at 298 K.

Amphoteric Substances

An amphoteric species is a chemical substance that possesses the ability to act as both an acid and a base. This dual nature allows them to either donate a proton (acting as an acid) or accept a proton (acting as a base), depending on the chemical environment.
Diagram

Characteristics and Reactions of Bases

Soluble bases are commonly referred to as alkalis. A key property of bases is their ability to neutralize acids, a reaction that typically produces water. When dissolved in water, bases release hydroxide (OH-) ions. Common examples of bases include:
    • Metal oxides and hydroxides (excluding insoluble compounds).
    • Ammonia (NH3).
    • Soluble carbonates (e.g., Na2CO3, K2CO3) and hydrogen carbonates (e.g., KHCO3).
The dissolution and reaction of these bases in water can be illustrated by the following equations:

K2O(s) + H2O(l) → 2K+(aq) + 2OH-(aq)

NH3(aq) + H2O(l) ⇌ NH4+(aq) + OH-(aq)

CO32-(aq) + H2O(l) ⇌ HCO3-(aq) + OH-(aq)

HCO3-(aq) ⇌ CO2(g) + OH-(aq)

2
Reactions of Acids

Introduction to Acid Reactions and Salt Formation

Acids are characterized by their ability to react with various substances, including metals, bases, and carbonates, to produce salts. A salt is defined as an ionic compound formed when the hydrogen ion of an acid is replaced by a metal ion or another positive ion. These reactions are fundamental in chemistry and are often categorized by the type of reactant involved. The formation of salts from acids and bases is a key concept, with the acid and base sometimes referred to as the "parent acid" and "parent base" of the resulting salt. There are three primary types of reactions where acids yield a salt: the reaction of an acid with a metal, an acid with a base, and an acid with a carbonate.
Diagram

Acid Reactions with Metals

When an acid reacts with a metal, the general equation is: Acid + Metal → Salt + Hydrogen gas. For instance, hydrochloric acid reacts with zinc to produce zinc chloride and hydrogen gas, as shown by the equation:
2HCl(aq) + Zn(s) → ZnCl2(aq) + H2(g). Similarly, sulfuric acid reacts with iron to form iron(II) sulfate and hydrogen gas: H2SO4(aq) + Fe(s) → FeSO4(aq) + H2(g).
Acetic acid, a weak acid, also reacts with magnesium to yield magnesium acetate and hydrogen gas:
2CH3COOH(aq) + Mg(s) → Mg(CH3COO)2(aq) + H2(g).
These reactions can also be represented by ionic equations, focusing on the species that undergo change. For example, the reaction between hydrochloric acid and zinc can be simplified to the net ionic equation:
2H+(aq) + Zn(s) → Zn2+(aq) + H2(g),
where chloride ions are spectator ions. Acids are known for their corrosive properties towards most metals, though the reactivity varies significantly among different metals. Group 1 metals, such as sodium and potassium, are highly reactive with acids, while some transition metals, like gold and platinum, exhibit much lower reactivity, which contributes to their value and resistance to corrosion.
Diagram

Acid Reactions with Bases (Neutralization)

The reaction between an acid and a base is commonly known as a neutralization reaction, and it typically produces a salt and water. The general equation for this type of reaction is: Acid + Base → Salt + Water. Examples include the reaction of hydrochloric acid with sodium hydroxide to form sodium chloride and water: HCl(aq) + NaOH(aq) → NaCl(aq) + H2O(l). Nitric acid reacts with ammonium hydroxide to produce ammonium nitrate and water:
HNO3(aq) + NH4OH(aq) → NH4NO3(aq) + H2O(l).
Acetic acid reacts with copper(II) oxide to form copper(II) acetate and water:
2CH3COOH(aq) + CuO(aq) → Cu(CH3COO)2(aq) + H2O(l).
All these neutralization reactions can be represented by a single common net ionic equation:
H+(aq) + OH-(aq) → H2O(l), which highlights the formation of water from hydrogen ions and hydroxide ions. Neutralization reactions are exothermic, meaning they release heat. The enthalpy of neutralization is defined as the enthalpy change that occurs when an acid and a base react to form one mole of water. Reactions between strong acids and strong bases typically have a high enthalpy of neutralization, approximately -57 kJmol-1, indicating a significant release of energy.

Acid Reactions with Carbonates

Acids react with carbonates to produce a salt, water, and carbon dioxide gas. The general equation for this reaction is: Acid + Carbonate → Salt + Water + Carbon Dioxide. For instance, hydrochloric acid reacts with calcium carbonate to yield calcium chloride, water, and carbon dioxide:
2HCl(aq) + CaCO3(s) → CaCl2(aq) + H2O(l) + CO2(g). 
Sulfuric acid reacts with sodium carbonate to form sodium sulfate, water, and carbon dioxide:
H2SO4(aq) + Na2CO3(aq) → Na2SO4(aq) + H2O(l) + CO2(g).
Similarly, acetic acid reacts with potassium hydrogen carbonate to produce potassium acetate, water, and carbon dioxide: CH3COOH(aq) + KHCO3(aq) → KCH
Diagram
3COO(aq) + H2O(l) + CO2(g).
The common net ionic equation for these reactions is:
2H+(aq) + CO32-(aq) → H2O(l) + CO2(g).
A characteristic feature of these reactions is the visible production of bubbles, known as effervescence, due to the release of carbon dioxide gas.

Brønsted-Lowry Theory of Acids and Bases

The Brønsted-Lowry theory provides a framework for understanding acid-base reactions by focusing on the transfer of protons (H+ ions). According to this theory, a Brønsted-Lowry acid is defined as a proton (H+) donor, while a Brønsted-Lowry base is a proton (H+) acceptor. It is important to note that the terms "H+" and "proton" are used interchangeably in this context, as a hydrogen ion consists solely of a proton. A classic example illustrating this theory is the reaction between hydrogen chloride and ammonia: HCl + NH3 ⇌ NH4+ + Cl-.
In this reaction, HCl donates a proton to NH3, making HCl the acid and NH3 the base.

Conjugate Acid-Base Pairs

In any Brønsted-Lowry acid-base reaction, a proton donor must always be paired with a proton acceptor; proton transfer does not occur in isolation. The general formula for such a reaction can be represented as: HA + B ⇌ A- + BH+. Here, HA is the acid that donates a proton, forming its conjugate base A-. Conversely, B is the base that accepts a proton, forming its conjugate acid BH+. A conjugate acid is defined as a species that can donate a proton, meaning it must be able to dissociate and release an H+ ion. A conjugate base is a species that can accept a proton, which implies it must possess a lone pair of electrons to bond with the incoming H+ ion. Consider the example of water reacting with a proton:
H2O(l) + H+(aq) ⇌ H3O+(aq).
In this reaction, H2O acts as a base, accepting a proton to form the hydronium ion, H3O+. Therefore, H3O+ is the conjugate acid of H2O, and H2O is the conjugate base of H3O+. The hydronium ion (H3O+) is always the actual form of hydrogen ions in an aqueous solution, although it is often conveniently written as H+(aq). A key principle of conjugate acid-base pairs is that a conjugate acid always possesses one more proton than its corresponding conjugate base.

Amphiprotic and Amphoteric Species

Some chemical species exhibit the unique ability to act as both acids and bases. Such species are termed amphiprotic if their dual nature involves the transfer of protons. An amphiprotic species can both donate and accept protons. It is important to distinguish amphiprotic from amphoteric; while all amphiprotic species are amphoteric, not all amphoteric species are amphiprotic. Amphoteric refers to any species that can act as an acid and a base, regardless of whether proton transfer is involved. Water is a prime example of an amphiprotic and amphoteric substance. It can act as a base by accepting a proton, as seen in its reaction with ammonia: NH3 + H2O ⇌ NH4+ + OH-.
In this case, water donates a proton to ammonia, making water the acid. Conversely, water can act as an acid by donating a proton, as demonstrated in its reaction with acetic acid:
CH3COOH + H2O ⇌ CH3COO- + H3O+.
Here, water accepts a proton from acetic acid, making water the base.
Species Can Act As Example Reaction (as acid) Example Reaction (as base)
H2O Acid and Base NH3 + H2O ⇌ NH4+ + OH- CH3COOH + H2O ⇌ CH3COO- + H3O+
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Strong vs. Weak

Defining Acid and Base Strength by Dissociation

The fundamental distinction between strong and weak acids and bases lies in the extent of their dissociation when dissolved in a solution. According to the Arrhenius definition, acids are substances that produce hydrogen ions (H+) in solution, while bases produce hydroxide ions (OH-). The degree to which these substances ionize determines their strength.

Characteristics of Strong and Weak Acids

Strong acids are characterized by their complete dissociation in an aqueous solution, meaning they exist almost entirely as ions. This makes them excellent proton donors. For instance, when a generic strong acid, HA, is dissolved in water, it reacts completely to form its conjugate base, A-, and hydronium ions, H3O+, as shown in the following reaction: HA(aq) + H2O(l) → A-(aq) + H3O+(aq)
 A classic example is hydrochloric acid: HCl(aq) + H2O(l) → H3O+(aq) + Cl-(aq)
 In this reaction, HCl acts as the strong acid, H2O as the base, H3O+ as the conjugate acid, and Cl- as the conjugate base. Conversely, weak acids dissociate only partially in solution, establishing an equilibrium where the undissociated molecular form predominates. They are considered weak proton donors. For example, acetic acid (CH3COOH) in water sets up an equilibrium:
 CH3COOH(aq) + H2O(l) ⇌ H3O+(aq) + CH3COO-(aq)
 Here, CH3COOH is the weak acid, H2O is the base, H3O+ is the conjugate acid, and CH3COO- is the conjugate base. A key characteristic of weak acids is that they form stronger conjugate bases. In the equilibrium for a weak acid, the equilibrium position lies predominantly to the left, favoring the undissociated acid.

Characteristics of Strong and Weak Bases

Similar to acids, the strength of a base is determined by its dissociation. Strong bases dissociate fully in solution, existing entirely as ions, and are excellent proton acceptors. A generic strong base, BOH, dissociates as follows: BOH(aq) → B+(aq) + OH-(aq)
 Sodium hydroxide (NaOH) is a common example: NaOH(aq) → Na+(aq) + OH-(aq)
 Weak bases, on the other hand, dissociate only partially, forming an equilibrium mixture where the undissociated form is dominant. They are weak proton acceptors. Ammonia (NH3) reacting with water illustrates this: NH3(aq) + H2O(l) ⇌ NH4+(aq) + OH-(aq)
In this reaction, NH3 is the weak base, H2O is the acid, NH4+ is the conjugate acid, and OH- is the conjugate base. It is important to note that weak bases form stronger conjugate acids. For weak bases, the equilibrium also lies to the left, indicating that the undissociated base is the predominant species. It is crucial not to confuse the strength of an acid or base with its concentration; a strong acid or base can still be diluted to a low concentration.

Prevalence of Weak Acids and Bases

Weak acids and bases are very common in chemistry, particularly in organic chemistry. Many organic acids and bases are listed in section 21 of the IB Chemistry Data Booklet, highlighting their widespread occurrence and importance.
Diagram

Distinguishing Between Strong and Weak Acids and Bases

Diagram
Several experimental methods can be employed to distinguish between strong and weak acids and bases, provided that solutions of the same concentration are compared at the same temperature. These methods primarily rely on the differing concentrations of ions produced by strong versus weak electrolytes. One effective method is measuring electrical conductivity. Strong acids and bases, due to their complete dissociation, produce a higher concentration of ions in solution, leading to significantly higher electrical conductivity compared to weak acids and bases of the same concentration. This can be readily measured using a conductivity meter. Another distinguishing factor is the rate of reaction. Strong acids and bases will generally react at a faster rate than weak acids and bases of the same concentration, as the higher concentration of H+ or OH- ions facilitates quicker reaction kinetics. However, quantifying this difference can be challenging. For example, the reaction of hydrochloric acid (a strong acid) with magnesium metal will be much more vigorous than the reaction of acetic acid (a weak acid) with magnesium, even if both acid solutions have the same initial concentration. Finally, pH measurements provide a clear distinction. Stronger acids will exhibit a lower pH value, indicating a higher concentration of H3O+ ions, while stronger bases will have a higher pH value, reflecting a higher concentration of OH- ions.
Property Strong Acid/Base Weak Acid/Base
Dissociation Complete Partial (equilibrium)
Ion Concentration High Low
Electrical Conductivity High Low
Rate of Reaction Fast Slow
Conjugate Strength Weak conjugate Strong conjugate
pH (for acids) Very low Higher (but still acidic)
pH (for bases) Very high Lower (but still basic)
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Titrations & pH

Indicators for Distinguishing Acids and Bases

Indicators are chemical substances that reversibly change color depending on the concentration of hydrogen ions (H+) in a solution. They can be employed as aqueous solutions or absorbed onto test paper. This color change occurs because indicators are typically weak acids or bases whose conjugate forms possess distinct colors. The most widely recognized indicator is litmus, which exhibits a pink hue in acidic conditions and a blue hue in alkaline conditions. Additional indicators and their properties can be found in Section 22 of the IB Chemistry Data Booklet. A Universal Indicator is a blend of several indicators, designed to display multiple color changes across a broad spectrum of pH values, thereby indicating the approximate pH of a solution.
Indicator Color in acid Color in alkali
litmus pink blue
Methyl orange red yellow
phenolphthalein colorless pink
Diagram

Understanding Acid-Base Titrations

Acid-base titrations are analytical procedures that involve reacting a precisely measured volume of one solution with another solution, which is gradually added until the equivalence point is reached. The equivalence point signifies the point at which the acid and base have completely neutralized each other. Indicators play a crucial role in titrations by signaling the equivalence point through a distinct color change. It is important to note that the color changes associated with indicators are not universally fixed (e.g., acid always pink, alkali always blue); rather, they are specific to each indicator.
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Acid Deposition

Understanding Acid Deposition: Wet and Dry Processes

Acid deposition encompasses all processes by which acidic components, whether as precipitates or gases, are removed from the atmosphere and deposited onto the Earth's surface. There are two primary types: wet acid deposition and dry acid deposition. Wet acid deposition occurs when acidic substances fall to the ground as aqueous precipitates, including rain, snow, sleet, hail, fog, mist, and dew. In contrast, dry acid deposition involves acidifying particles and gases settling on the ground as dust and smoke, which then dissolve in water to form acids. It is important to note that all rainwater is inherently acidic due to the presence of dissolved carbon dioxide, which reacts with water to produce carbonic acid, as shown in the following equilibrium: H2O(l) ﹢ CO2(g) ⇌ H2CO3(aq) This carbonic acid then partially dissociates, releasing hydrogen ions: H2CO3(aq) ⇌ H+(aq) ﹢ HCO3-(aq) This natural acidity of rainwater can react with calcium carbonate found in limestone, forming soluble calcium hydrogencarbonate. This process leads to erosion and is a significant factor in the formation of caves in limestone regions.
Diagram

Defining Acid Rain and Its Primary Contributors

While all rainwater is naturally acidic due to dissolved carbon dioxide, the term "acid rain" specifically refers to solutions with a pH value less than 5.6, indicating the presence of additional acids beyond carbonic acid. The main contributors to this heightened acidity are pollutants, primarily oxides of sulfur and nitrogen, which are released into the atmosphere from various human activities.
Diagram

The Role of Sulfur Oxides in Acid Deposition

Sulfur dioxide (SO2) is a major atmospheric pollutant contributing to acid deposition. It is primarily generated from the combustion of fossil fuels, such as coal and oil, and is also released during the smelting process, which involves extracting metals from their ores. Approximately 50% of global annual SO2 emissions originate from coal combustion. The initial reaction involves the burning of sulfur present in these fuels: S(s) ﹢ O2(g) → SO2(g)
 Once in the atmosphere, sulfur dioxide can dissolve in water to form sulfurous acid: H2O(l) ﹢ SO2(g) → H2SO3(aq)
 Furthermore, SO2 can undergo oxidation to form sulfur trioxide (SO3), which then readily dissolves in water to produce sulfuric acid, a much stronger acid:
 2SO2(g) ﹢ O2(g) → 2SO3(g) H2O(l) ﹢ SO3(g) → H2SO4(aq)
 Hydroxyl free radicals (ᐧHO), which are formed in the atmosphere through reactions between water and oxygen or ozone, can also play a role in the oxidation of SO2:
 ᐧHO ﹢ SO2 → ᐧHOSO2 ᐧHOSO2 ﹢ O2 → ᐧHO2 ﹢ SO3

The Contribution of Nitrogen Oxides to Acid Deposition

Nitrogen oxides are another significant group of pollutants contributing to acid deposition. Nitrogen monoxide (NO) is predominantly produced in internal combustion engines, where high temperatures cause atmospheric nitrogen and oxygen to react:
 N2(g) ﹢ O2(g) → 2NO(g)
 Nitrogen dioxide (NO2), a brown gas, can also be formed through a similar reaction or by the oxidation of nitrogen monoxide:
 N2(g) ﹢ 2O2(g) → 2NO2(g)
2NO(g) ﹢ O2(g) → 2NO2(g)
 When nitrogen dioxide dissolves in water, it forms a mixture of nitrous acid and nitric acid:
 H2O(l) ﹢ 2NO2(g) → HNO2(aq) ﹢ HNO3(aq)
 Additionally, NO2 can be further oxidized to form nitric acid:
 H2O(l) ﹢ 4NO2(g) ﹢ O2(g) → 4HNO3(aq)
 Hydroxyl free radicals also contribute to the formation of both nitrous and nitric acid through reactions with nitrogen oxides: ᐧHO ﹢ NO → HNO2 ᐧHO ﹢ NO2 → HNO3
Diagram

Detrimental Effects of Acid Deposition on Materials and Plant Life

Acid deposition has a wide range of damaging effects on both natural and man-made environments. Its impact on materials is particularly evident in the degradation of building structures. Marble and limestone, both forms of calcium carbonate, are highly susceptible. Sulfur dioxide and sulfuric acid react with calcium carbonate to form calcium sulfate (CaSO4). Since calcium sulfate is soluble, it either washes away or flakes off, leading to significant erosion of these materials. Similarly, nitric acid can react with limestone to produce soluble calcium nitrate, further contributing to material degradation. Acid deposition also corrodes metals such as iron and aluminum, forming salts that damage metallic structures like bridges, railroad tracks, and vehicles. The impact on plant life is equally severe. Acid rain can cause slower growth, injury, or even death of plants. It leaches essential soluble minerals, such as magnesium, calcium, and potassium, from the soil, depriving plants of vital nutrients. Furthermore, acid rain can trigger the release of toxic substances, such as aluminum ions, from soil minerals. Dry deposition, in the form of acidic particles, can physically block the pores on plant leaves, hindering gas exchange. Forests in hilly regions are particularly vulnerable as they are frequently enveloped by acidic clouds, leading to prolonged exposure.
Diagram

Adverse Effects of Acid Deposition on Aquatic Ecosystems and Human Health

The consequences of acid deposition extend significantly to aquatic environments and human health. Acid rain can lead to the acidification of lakes, rendering them "dead" and unable to support life due to decreasing pH values. Many fish species cannot survive in water with a pH below 5. When pH levels drop below 4, aluminum ions are leached out of aluminum hydroxide, which is stored in rocks. These aluminum ions are highly toxic to aquatic life, interfering with fish's ability to take in oxygen. Additionally, the presence of nitrates in acid rain can cause over-fertilization of water bodies, a phenomenon known as eutrophication. This leads to excessive algal blooms, which subsequently deplete oxygen levels in the water, harming other aquatic organisms. Regarding human health, the components of acid rain can react in the atmosphere to form fine sulfate and nitrate particles, known as particulates. These particulates can travel long distances and, when inhaled, irritate the eyes and respiratory tract, exacerbating or causing conditions such as asthma, bronchitis, and emphysema. The release of toxic metal ions when acid rain reacts with metal structures also poses a potential health risk to humans.
Diagram

Strategies for Mitigating Sulfur Dioxide Emissions

Addressing acid deposition requires a multi-faceted approach, with significant efforts directed towards reducing the emissions of sulfur dioxide (SO2). These strategies can be broadly categorized into pre-combustion and post-combustion methods. Pre-combustion methods focus on reducing or removing sulfur from coal and oil before they are burned. An example is hydrodesulfurization (HDS), a process that removes sulfur from petroleum by reacting it with hydrogen to form hydrogen sulfide (H2S). Since H2S is a toxic gas, it is captured and subsequently utilized in the production of sulfuric acid, thus preventing its release into the atmosphere. Post-combustion methods involve treating the exhaust gases after combustion to remove pollutants. Flue-gas desulfurization is a highly effective technique that can remove up to 90% of SO2 from the flue gas emitted by coal-fired power stations before it is released. In this process, calcium oxide (CaO) or calcium carbonate (CaCO3) reacts with SO2 to form calcium sulfate (CaSO4), effectively scrubbing the sulfur dioxide from the exhaust.

Strategies for Mitigating Nitrogen Oxide Emissions and Broader Solutions

Reducing nitrogen oxide (NOx) emissions is another critical aspect of combating acid deposition. Several strategies are employed to achieve this:
  • Catalytic Converters in Vehicles: These devices are installed in vehicle exhaust systems. Hot exhaust gases are mixed with air and passed over a catalyst, typically made of platinum or palladium. This process converts toxic emissions, including nitrogen oxides, into less harmful substances such as carbon dioxide and nitrogen gas.
  • Lower Temperature Combustion: By recirculating exhaust gases back into the engine, the combustion temperature can be lowered. This reduction in temperature decreases the formation of nitrogen oxides, as their production is highly dependent on high temperatures.
Beyond these specific emission reduction techniques, broader solutions are essential for a sustainable future. These include lowering the overall demand for fossil fuels, implementing more efficient energy transfer systems, promoting greater use of public transportation, and transitioning to renewable energy sources. Finally, the restoration of ecosystems damaged by acid rain is a long-term and challenging process. One common method for mitigating the acidity in affected areas, particularly lakes and soils, is to add calcium oxide (CaO) or calcium hydroxide (Ca(OH)2) to neutralize the acids present.